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Items: 8

1.

Widespread global peatland establishment and persistence over the last 130,000 y.

Treat CC, Kleinen T, Broothaerts N, Dalton AS, Dommain R, Douglas TA, Drexler JZ, Finkelstein SA, Grosse G, Hope G, Hutchings J, Jones MC, Kuhry P, Lacourse T, Lähteenoja O, Loisel J, Notebaert B, Payne RJ, Peteet DM, Sannel ABK, Stelling JM, Strauss J, Swindles GT, Talbot J, Tarnocai C, Verstraeten G, Williams CJ, Xia Z, Yu Z, Väliranta M, Hättestrand M, Alexanderson H, Brovkin V.

Proc Natl Acad Sci U S A. 2019 Mar 12;116(11):4822-4827. doi: 10.1073/pnas.1813305116. Epub 2019 Feb 25.

2.

Successional change of testate amoeba assemblages along a space-for-time sequence of peatland development.

Zhang H, Väliranta M, Amesbury MJ, Charman DJ, Laine A, Tuittila ES.

Eur J Protistol. 2018 Oct;66:36-47. doi: 10.1016/j.ejop.2018.07.003. Epub 2018 Jul 24.

PMID:
30075360
3.

Abrupt high-latitude climate events and decoupled seasonal trends during the Eemian.

Salonen JS, Helmens KF, Brendryen J, Kuosmanen N, Väliranta M, Goring S, Korpela M, Kylander M, Philip A, Plikk A, Renssen H, Luoto M.

Nat Commun. 2018 Jul 20;9(1):2851. doi: 10.1038/s41467-018-05314-1.

4.

Warm summers during the Younger Dryas cold reversal.

Schenk F, Väliranta M, Muschitiello F, Tarasov L, Heikkilä M, Björck S, Brandefelt J, Johansson AV, Näslund JO, Wohlfarth B.

Nat Commun. 2018 Apr 24;9(1):1634. doi: 10.1038/s41467-018-04071-5.

5.

First physical evidence for forested environment in the Arctic during MIS 3.

Sarala P, Väliranta M, Eskola T, Vaikutiené G.

Sci Rep. 2016 Jul 1;6:29054. doi: 10.1038/srep29054.

6.

The extent and meaning of hybridization and introgression between Siberian spruce (Picea obovata) and Norway spruce (Picea abies): cryptic refugia as stepping stones to the west?

Tsuda Y, Chen J, Stocks M, Källman T, Sønstebø JH, Parducci L, Semerikov V, Sperisen C, Politov D, Ronkainen T, Väliranta M, Vendramin GG, Tollefsrud MM, Lascoux M.

Mol Ecol. 2016 Jun;25(12):2773-89. doi: 10.1111/mec.13654. Epub 2016 May 18.

PMID:
27087633
7.

Plant macrofossil evidence for an early onset of the Holocene summer thermal maximum in northernmost Europe.

Väliranta M, Salonen JS, Heikkilä M, Amon L, Helmens K, Klimaschewski A, Kuhry P, Kultti S, Poska A, Shala S, Veski S, Birks HH.

Nat Commun. 2015 Apr 10;6:6809. doi: 10.1038/ncomms7809.

8.

Proxy comparison in ancient peat sediments: pollen, macrofossil and plant DNA.

Parducci L, Väliranta M, Salonen JS, Ronkainen T, Matetovici I, Fontana SL, Eskola T, Sarala P, Suyama Y.

Philos Trans R Soc Lond B Biol Sci. 2015 Jan 19;370(1660):20130382. doi: 10.1098/rstb.2013.0382.

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